Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism
- Autores
- Aragon, Eugenio; Gonzalez, Pablo Diego; AGUILERA, Emilia Yolanda; Cavarozzi, Claudia Ernestina; Llambias, Eduardo Jorge; Rivalenti, Giorgio
- Año de publicación
- 2003
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Andesitas Alvar Formation is part of the large Jurassic volcanic province of Patagonia (southern South America) that, in Jurassic time, participated in the disassembling of Gondwana in a tensional-transtensional regime with large-scale half-grabens. This large igneous province contains alkaline and calc-alkaline series of andesite-trachyte, trachyte-rhyolite, and andesite-dacite trends. Four-phase experimental diagrams of Qz-Or-Ab-An and Ab-An-Ol-Di correlate with the TAS diagram and explain the Andesitas Alvar Formation's sodium-rich andesite-trachyte, which evolved through a thermal divide edge. This alkaline set initially included the paragenesis olivine-plagioclase-diopsidic augite, which was later replaced by hornblende-plagioclase-diopsidic augite. The andesite-trachyte trend is saturated in silica and rich in sodium and alumina. Diopsidic augite, plagioclase, and hornblende crystals are reverse zoned in magnesium, iron, calcium, and sodium, so the sodium-rich cores of plagioclase are not due to contamination, and the magmas mix several batches of partial melts of basic rock. Crystallization temperatures and pressures show that magma chamber emplacement and thermal reversal took place mainly at 4 kb. This is interpreted as the emplacement of collecting chambers at the brittle-ductile transition in the crust, where mixing and crystallization took place, followed by rapid extrusion in a transtensional tectonic environment. © 2003 Elsevier Ltd. All rights reserved.
Fil: Aragon, Eugenio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Gonzalez, Pablo Diego. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: AGUILERA, Emilia Yolanda. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; Argentina
Fil: Cavarozzi, Claudia Ernestina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Llambias, Eduardo Jorge. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Rivalenti, Giorgio. Universita degli Studi di Modena; Italia - Materia
-
Alkaline
Andesite
Jurassic
Thermal Divide
Trachyte - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/75141
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Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanismAragon, EugenioGonzalez, Pablo DiegoAGUILERA, Emilia YolandaCavarozzi, Claudia ErnestinaLlambias, Eduardo JorgeRivalenti, GiorgioAlkalineAndesiteJurassicThermal DivideTrachytehttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Andesitas Alvar Formation is part of the large Jurassic volcanic province of Patagonia (southern South America) that, in Jurassic time, participated in the disassembling of Gondwana in a tensional-transtensional regime with large-scale half-grabens. This large igneous province contains alkaline and calc-alkaline series of andesite-trachyte, trachyte-rhyolite, and andesite-dacite trends. Four-phase experimental diagrams of Qz-Or-Ab-An and Ab-An-Ol-Di correlate with the TAS diagram and explain the Andesitas Alvar Formation's sodium-rich andesite-trachyte, which evolved through a thermal divide edge. This alkaline set initially included the paragenesis olivine-plagioclase-diopsidic augite, which was later replaced by hornblende-plagioclase-diopsidic augite. The andesite-trachyte trend is saturated in silica and rich in sodium and alumina. Diopsidic augite, plagioclase, and hornblende crystals are reverse zoned in magnesium, iron, calcium, and sodium, so the sodium-rich cores of plagioclase are not due to contamination, and the magmas mix several batches of partial melts of basic rock. Crystallization temperatures and pressures show that magma chamber emplacement and thermal reversal took place mainly at 4 kb. This is interpreted as the emplacement of collecting chambers at the brittle-ductile transition in the crust, where mixing and crystallization took place, followed by rapid extrusion in a transtensional tectonic environment. © 2003 Elsevier Ltd. All rights reserved.Fil: Aragon, Eugenio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Gonzalez, Pablo Diego. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: AGUILERA, Emilia Yolanda. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; ArgentinaFil: Cavarozzi, Claudia Ernestina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Llambias, Eduardo Jorge. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Rivalenti, Giorgio. Universita degli Studi di Modena; ItaliaPergamon-Elsevier Science Ltd2003-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/75141Aragon, Eugenio; Gonzalez, Pablo Diego; AGUILERA, Emilia Yolanda; Cavarozzi, Claudia Ernestina; Llambias, Eduardo Jorge; et al.; Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 16; 3; 12-2003; 91-1030895-9811CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/S0895-9811(03)00046-4info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0895981103000464info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:46:21Zoai:ri.conicet.gov.ar:11336/75141instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:46:21.953CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism |
title |
Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism |
spellingShingle |
Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism Aragon, Eugenio Alkaline Andesite Jurassic Thermal Divide Trachyte |
title_short |
Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism |
title_full |
Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism |
title_fullStr |
Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism |
title_full_unstemmed |
Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism |
title_sort |
Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism |
dc.creator.none.fl_str_mv |
Aragon, Eugenio Gonzalez, Pablo Diego AGUILERA, Emilia Yolanda Cavarozzi, Claudia Ernestina Llambias, Eduardo Jorge Rivalenti, Giorgio |
author |
Aragon, Eugenio |
author_facet |
Aragon, Eugenio Gonzalez, Pablo Diego AGUILERA, Emilia Yolanda Cavarozzi, Claudia Ernestina Llambias, Eduardo Jorge Rivalenti, Giorgio |
author_role |
author |
author2 |
Gonzalez, Pablo Diego AGUILERA, Emilia Yolanda Cavarozzi, Claudia Ernestina Llambias, Eduardo Jorge Rivalenti, Giorgio |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
Alkaline Andesite Jurassic Thermal Divide Trachyte |
topic |
Alkaline Andesite Jurassic Thermal Divide Trachyte |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The Andesitas Alvar Formation is part of the large Jurassic volcanic province of Patagonia (southern South America) that, in Jurassic time, participated in the disassembling of Gondwana in a tensional-transtensional regime with large-scale half-grabens. This large igneous province contains alkaline and calc-alkaline series of andesite-trachyte, trachyte-rhyolite, and andesite-dacite trends. Four-phase experimental diagrams of Qz-Or-Ab-An and Ab-An-Ol-Di correlate with the TAS diagram and explain the Andesitas Alvar Formation's sodium-rich andesite-trachyte, which evolved through a thermal divide edge. This alkaline set initially included the paragenesis olivine-plagioclase-diopsidic augite, which was later replaced by hornblende-plagioclase-diopsidic augite. The andesite-trachyte trend is saturated in silica and rich in sodium and alumina. Diopsidic augite, plagioclase, and hornblende crystals are reverse zoned in magnesium, iron, calcium, and sodium, so the sodium-rich cores of plagioclase are not due to contamination, and the magmas mix several batches of partial melts of basic rock. Crystallization temperatures and pressures show that magma chamber emplacement and thermal reversal took place mainly at 4 kb. This is interpreted as the emplacement of collecting chambers at the brittle-ductile transition in the crust, where mixing and crystallization took place, followed by rapid extrusion in a transtensional tectonic environment. © 2003 Elsevier Ltd. All rights reserved. Fil: Aragon, Eugenio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: Gonzalez, Pablo Diego. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: AGUILERA, Emilia Yolanda. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; Argentina Fil: Cavarozzi, Claudia Ernestina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: Llambias, Eduardo Jorge. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: Rivalenti, Giorgio. Universita degli Studi di Modena; Italia |
description |
The Andesitas Alvar Formation is part of the large Jurassic volcanic province of Patagonia (southern South America) that, in Jurassic time, participated in the disassembling of Gondwana in a tensional-transtensional regime with large-scale half-grabens. This large igneous province contains alkaline and calc-alkaline series of andesite-trachyte, trachyte-rhyolite, and andesite-dacite trends. Four-phase experimental diagrams of Qz-Or-Ab-An and Ab-An-Ol-Di correlate with the TAS diagram and explain the Andesitas Alvar Formation's sodium-rich andesite-trachyte, which evolved through a thermal divide edge. This alkaline set initially included the paragenesis olivine-plagioclase-diopsidic augite, which was later replaced by hornblende-plagioclase-diopsidic augite. The andesite-trachyte trend is saturated in silica and rich in sodium and alumina. Diopsidic augite, plagioclase, and hornblende crystals are reverse zoned in magnesium, iron, calcium, and sodium, so the sodium-rich cores of plagioclase are not due to contamination, and the magmas mix several batches of partial melts of basic rock. Crystallization temperatures and pressures show that magma chamber emplacement and thermal reversal took place mainly at 4 kb. This is interpreted as the emplacement of collecting chambers at the brittle-ductile transition in the crust, where mixing and crystallization took place, followed by rapid extrusion in a transtensional tectonic environment. © 2003 Elsevier Ltd. All rights reserved. |
publishDate |
2003 |
dc.date.none.fl_str_mv |
2003-12 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/75141 Aragon, Eugenio; Gonzalez, Pablo Diego; AGUILERA, Emilia Yolanda; Cavarozzi, Claudia Ernestina; Llambias, Eduardo Jorge; et al.; Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 16; 3; 12-2003; 91-103 0895-9811 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/75141 |
identifier_str_mv |
Aragon, Eugenio; Gonzalez, Pablo Diego; AGUILERA, Emilia Yolanda; Cavarozzi, Claudia Ernestina; Llambias, Eduardo Jorge; et al.; Thermal divide andesites - trachytes, petrologic evidence, and implications from Jurassic north Patagonian massif alkaline volcanism; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 16; 3; 12-2003; 91-103 0895-9811 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1016/S0895-9811(03)00046-4 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0895981103000464 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf application/pdf application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Pergamon-Elsevier Science Ltd |
publisher.none.fl_str_mv |
Pergamon-Elsevier Science Ltd |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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1844614504855371776 |
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13.070432 |